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- W2964702751 abstract "This study presents new zircon U–Pb ages, Sr–Nd–Hf isotopic data, and whole‐rock geochemical data obtained from the Early Cretaceous volcanic rocks from the north‐western Great Xing'an Range, Northeast China, to constrain the late Mesozoic magmatism and geodynamic setting of this region, which is located in the eastern segment of the Central Asian Orogenic Belt (CAOB). Zircon U–Pb age determinations show that the studied samples formed at 124–114 Ma with an Early Cretaceous magmatic event produced voluminous felsic and minor mafic volcanic rocks. The mafic rocks are dominantly basalt and basaltic andesite, with relatively low SiO 2 contents (49.88–56.64 wt.%). These rocks are enriched in Th, U, large‐ion lithophile elements (LILE; e.g., Rb, Ba, and K) and light rare‐earth elements (REEs), and depleted in high‐field‐strength elements (HFSE; e.g., Nb, Ta, and Ti) and heavy REEs (Yb and Lu). The rocks have εNd(t) values of 0.44–0.75 and initial 87 Sr/ 86 Sr ratio of 0.70499–0.70548. These results indicate that the mafic rocks were derived from the partial melting of enriched lithospheric mantle that had been previously metasomatized by subduction‐related fluids and experienced variable amounts of fractional crystallization and moderate crustal contamination. In contrast to the mafic rocks, the felsic rocks are dominantly peraluminous trachytes, rhyolites, and dacites with high SiO 2 contents and low MgO contents. These felsic rocks display enriched and variable concentrations of LILEs and REEs, show negative Eu anomalies, and have ε Hf (t) values of +2.6 to +8.3 with T DM2 ages of 1,014–655 Ma, indicating they were derived from partial melting of juvenile crustal materials. These Early Cretaceous igneous rock assemblages record a post‐collisional lithospheric extensional setting resulting from the closure of the Mongol–Okhotsk Ocean, consistent with the results of previous studies on the contemporaneous tectono‐magmatic activities in NE China." @default.
- W2964702751 created "2019-08-13" @default.
- W2964702751 creator A5005344083 @default.
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- W2964702751 creator A5049780306 @default.
- W2964702751 creator A5055082070 @default.
- W2964702751 creator A5072681445 @default.
- W2964702751 date "2019-07-28" @default.
- W2964702751 modified "2023-10-14" @default.
- W2964702751 title "Petrogenesis and tectonic implications of Early Cretaceous volcanic rocks from the Shanghulin Basin within the north‐western Great Xing'an Range, NE China: Constraints from geochronology and geochemistry" @default.
- W2964702751 cites W1051026135 @default.
- W2964702751 cites W1104249897 @default.
- W2964702751 cites W1587780337 @default.
- W2964702751 cites W183765136 @default.
- W2964702751 cites W1871734886 @default.
- W2964702751 cites W1964038242 @default.
- W2964702751 cites W1964296772 @default.
- W2964702751 cites W1964617878 @default.
- W2964702751 cites W1965917434 @default.
- W2964702751 cites W1967827341 @default.
- W2964702751 cites W1967993347 @default.
- W2964702751 cites W1969859799 @default.
- W2964702751 cites W1971000065 @default.
- W2964702751 cites W1971616481 @default.
- W2964702751 cites W1977650828 @default.
- W2964702751 cites W1979694545 @default.
- W2964702751 cites W1979705656 @default.
- W2964702751 cites W1981207838 @default.
- W2964702751 cites W1982221118 @default.
- W2964702751 cites W1987907556 @default.
- W2964702751 cites W1988317790 @default.
- W2964702751 cites W1988557437 @default.
- W2964702751 cites W1995897602 @default.
- W2964702751 cites W1997070082 @default.
- W2964702751 cites W1997705537 @default.
- W2964702751 cites W2003323528 @default.
- W2964702751 cites W2004195387 @default.
- W2964702751 cites W2005781914 @default.
- W2964702751 cites W2008127132 @default.
- W2964702751 cites W2011607179 @default.
- W2964702751 cites W2017222910 @default.
- W2964702751 cites W2020304604 @default.
- W2964702751 cites W2021987309 @default.
- W2964702751 cites W2022805129 @default.
- W2964702751 cites W2024070503 @default.
- W2964702751 cites W2026313871 @default.
- W2964702751 cites W2032006288 @default.
- W2964702751 cites W2033127801 @default.
- W2964702751 cites W2035003573 @default.
- W2964702751 cites W2035056660 @default.
- W2964702751 cites W2037708864 @default.
- W2964702751 cites W2039405518 @default.
- W2964702751 cites W2039511246 @default.
- W2964702751 cites W2039872199 @default.
- W2964702751 cites W2044620880 @default.
- W2964702751 cites W2045300556 @default.
- W2964702751 cites W2049907150 @default.
- W2964702751 cites W2050360542 @default.
- W2964702751 cites W2051581312 @default.
- W2964702751 cites W2052343049 @default.
- W2964702751 cites W2053514714 @default.
- W2964702751 cites W2054590577 @default.
- W2964702751 cites W2054765896 @default.
- W2964702751 cites W2055112659 @default.
- W2964702751 cites W2059027044 @default.
- W2964702751 cites W2061837047 @default.
- W2964702751 cites W2068038089 @default.
- W2964702751 cites W2068291176 @default.
- W2964702751 cites W2072680255 @default.
- W2964702751 cites W2077149306 @default.
- W2964702751 cites W2077214987 @default.
- W2964702751 cites W2078105240 @default.
- W2964702751 cites W2080404285 @default.
- W2964702751 cites W2081673195 @default.
- W2964702751 cites W2087576009 @default.
- W2964702751 cites W2087795440 @default.
- W2964702751 cites W2089096123 @default.
- W2964702751 cites W2090206242 @default.
- W2964702751 cites W2092440925 @default.
- W2964702751 cites W2108056426 @default.
- W2964702751 cites W2108971421 @default.
- W2964702751 cites W2119424315 @default.
- W2964702751 cites W2119438235 @default.
- W2964702751 cites W2126127241 @default.
- W2964702751 cites W2127922409 @default.
- W2964702751 cites W2127994322 @default.
- W2964702751 cites W2138522501 @default.
- W2964702751 cites W2145898590 @default.
- W2964702751 cites W2158970693 @default.
- W2964702751 cites W2162457106 @default.
- W2964702751 cites W2170868101 @default.
- W2964702751 cites W2229174120 @default.
- W2964702751 cites W2325514473 @default.
- W2964702751 cites W2331566847 @default.
- W2964702751 cites W2353796300 @default.
- W2964702751 cites W2414721512 @default.
- W2964702751 cites W2493148478 @default.
- W2964702751 cites W2528431995 @default.